Skip to content
  • Home
  • Categories
    • Geology
    • Geography
    • Space and Astronomy
  • About
    • Privacy Policy
  • About
  • Privacy Policy
Our Planet TodayAnswers for geologist, scientists, spacecraft operators
  • Home
  • Categories
    • Geology
    • Geography
    • Space and Astronomy
  • About
    • Privacy Policy
on September 20, 2023

Quantifying Organic Material Content in SoilGrids: A Methodological Approach for Layer-wise Percentage Derivation

Soil

Contents:

  • Understanding SoilGrids and Organic Content
  • 1. SoilGrids: An Overview
  • 2. Data acquisition and calibration
  • 3. Geostatistical modeling and prediction
  • 4. Validation and uncertainty assessment
  • FAQs

Understanding SoilGrids and Organic Content

SoilGrids is a valuable resource for researchers, agronomists, and environmental scientists seeking to understand the properties and composition of soils around the world. A critical parameter in soil analysis is organic matter content, which provides insight into soil fertility, carbon sequestration potential, and overall soil health. In this article, we will explore the methods used to derive organic matter content as a percentage per layer in SoilGrids, shedding light on the scientific principles and data processing techniques involved.

1. SoilGrids: An Overview

Before discussing the methods used to estimate organic matter content in SoilGrids, it is important to understand the underlying framework. SoilGrids is a global soil information system developed by the International Institute for Applied Systems Analysis (IIASA) and the Joint Research Centre (JRC) of the European Commission. It uses state-of-the-art machine learning algorithms and advanced geostatistical techniques to predict soil properties based on a wide range of environmental covariates and soil observations.
Organic matter content in SoilGrids is estimated using a combination of remote sensing data, climate variables, and soil spectral measurements. These inputs, along with other ancillary data such as land cover and topography, are processed using sophisticated geostatistical models to produce high-resolution maps of soil properties. These maps are available in multiple layers representing different depths to provide a comprehensive understanding of the soil profile.

2. Data acquisition and calibration

In order to derive the organic matter content per layer in SoilGrids, a robust dataset of soil observations from multiple sources is required. These soil observations typically include measurements of organic carbon content, which serves as a proxy for organic matter content. The data collection process involves collecting soil samples from different locations around the world and analyzing them in laboratories to determine their organic carbon content.
The collected soil data are then combined with other environmental covariates, such as satellite imagery and climate data, to create a comprehensive dataset for model calibration. Advanced statistical techniques, including machine learning algorithms and regression models, are used to establish the relationships between the soil observations and the environmental covariates. This calibration phase aims to capture the complex spatial patterns and variability of organic matter content across different soil types and climatic conditions.

3. Geostatistical modeling and prediction

Once the calibration phase is complete, geostatistical modeling techniques are used to predict organic matter content in unsampled locations. Geostatistics is a field of study that combines statistical analysis with spatial relationships to model and predict the values of a target variable over a geographic area. In the context of SoilGrids, geostatistical models account for spatial autocorrelation and variation in organic matter content to produce accurate predictions.
Various geostatistical methods such as kriging, co-kriging, and regression kriging are used to interpolate organic matter values between sampled locations. These models take into account the spatial distance between sample points, the correlation structure of the data, and the influence of environmental covariates to estimate the organic matter content at unmeasured locations. The resulting predictions are then used to create high-resolution maps of organic matter content per layer in SoilGrids.

4. Validation and uncertainty assessment

To ensure the reliability and accuracy of the organic matter content estimates in SoilGrids, rigorous validation procedures are performed. Independent soil datasets not used during the calibration phase are used to assess the predictive performance of the models. Statistical metrics such as root mean square error (RMSE) and coefficient of determination (R²) are calculated to evaluate the agreement between the predicted values and the observed soil data.
In addition, uncertainty assessment techniques are used to quantify the uncertainty associated with the organic matter content estimates in SoilGrids. These techniques take into account the inherent variability in soil properties, the quality and quantity of available data, and the limitations of the modeling approaches. Uncertainty maps or confidence intervals are generated to provide users with a measure of the reliability and precision of the organic matter predictions.

In summary, the derivation of organic matter content per layer in SoilGrids involves a sophisticated combination of data collection, calibration, geostatistical modeling, and validation procedures. These methods enable the generation of high-resolution soil property maps that facilitate global soil analysis and support various applications in agriculture, environmental management, and land use planning. By understanding the underlying processes and uncertainties associated with SoilGrids, researchers and practitioners can make informed decisions and contribute to sustainable soil management practices.

FAQs

What method do I use to derive the organic material content (as a percentage) per layer in SoilGrids?

The organic material content in SoilGrids is derived using a combination of remote sensing data, machine learning algorithms, and ground observations.

How does remote sensing data contribute to deriving the organic material content in SoilGrids?

Remote sensing data, such as satellite imagery and aerial photographs, are used to capture information about the Earth’s surface. These data provide valuable insights into vegetation cover, land use, and other indicators related to organic material content in soil.

What role does machine learning play in deriving the organic material content in SoilGrids?

Machine learning algorithms are employed to analyze the remote sensing data and extract patterns and relationships between the data and the organic material content in soil. These algorithms are trained using a combination of ground observations and remotely sensed data to make accurate predictions across larger areas.

How are ground observations used in deriving the organic material content in SoilGrids?

Ground observations involve collecting samples of soil from various locations and measuring the organic material content through laboratory analysis. These observations provide reference data that are used to calibrate and validate the machine learning models, ensuring the accuracy of the derived organic material content in SoilGrids.

What are the advantages of using SoilGrids for deriving organic material content?

SoilGrids provide several advantages for deriving organic material content. These include the ability to estimate organic material content across large spatial extents with high resolution, the integration of diverse data sources for improved accuracy, and the continuous updates and availability of the data, allowing for temporal analysis and monitoring of changes in organic material content over time.

Recent

  • Exploring the Geological Features of Caves: A Comprehensive Guide
  • What Factors Contribute to Stronger Winds?
  • The Scarcity of Minerals: Unraveling the Mysteries of the Earth’s Crust
  • How Faster-Moving Hurricanes May Intensify More Rapidly
  • Adiabatic lapse rate
  • Exploring the Feasibility of Controlled Fractional Crystallization on the Lunar Surface
  • The Greenhouse Effect: How Rising Atmospheric CO2 Drives Global Warming
  • Examining the Feasibility of a Water-Covered Terrestrial Surface
  • What is an aurora called when viewed from space?
  • Measuring the Greenhouse Effect: A Systematic Approach to Quantifying Back Radiation from Atmospheric Carbon Dioxide
  • Asymmetric Solar Activity Patterns Across Hemispheres
  • Unraveling the Distinction: GFS Analysis vs. GFS Forecast Data
  • The Role of Longwave Radiation in Ocean Warming under Climate Change
  • Esker vs. Kame vs. Drumlin – what’s the difference?

Categories

  • English
  • Deutsch
  • Français
  • Home
  • About
  • Privacy Policy

Copyright Our Planet Today 2025

We use cookies on our website to give you the most relevant experience by remembering your preferences and repeat visits. By clicking “Accept”, you consent to the use of ALL the cookies.
Do not sell my personal information.
Cookie SettingsAccept
Manage consent

Privacy Overview

This website uses cookies to improve your experience while you navigate through the website. Out of these, the cookies that are categorized as necessary are stored on your browser as they are essential for the working of basic functionalities of the website. We also use third-party cookies that help us analyze and understand how you use this website. These cookies will be stored in your browser only with your consent. You also have the option to opt-out of these cookies. But opting out of some of these cookies may affect your browsing experience.
Necessary
Always Enabled
Necessary cookies are absolutely essential for the website to function properly. These cookies ensure basic functionalities and security features of the website, anonymously.
CookieDurationDescription
cookielawinfo-checkbox-analytics11 monthsThis cookie is set by GDPR Cookie Consent plugin. The cookie is used to store the user consent for the cookies in the category "Analytics".
cookielawinfo-checkbox-functional11 monthsThe cookie is set by GDPR cookie consent to record the user consent for the cookies in the category "Functional".
cookielawinfo-checkbox-necessary11 monthsThis cookie is set by GDPR Cookie Consent plugin. The cookies is used to store the user consent for the cookies in the category "Necessary".
cookielawinfo-checkbox-others11 monthsThis cookie is set by GDPR Cookie Consent plugin. The cookie is used to store the user consent for the cookies in the category "Other.
cookielawinfo-checkbox-performance11 monthsThis cookie is set by GDPR Cookie Consent plugin. The cookie is used to store the user consent for the cookies in the category "Performance".
viewed_cookie_policy11 monthsThe cookie is set by the GDPR Cookie Consent plugin and is used to store whether or not user has consented to the use of cookies. It does not store any personal data.
Functional
Functional cookies help to perform certain functionalities like sharing the content of the website on social media platforms, collect feedbacks, and other third-party features.
Performance
Performance cookies are used to understand and analyze the key performance indexes of the website which helps in delivering a better user experience for the visitors.
Analytics
Analytical cookies are used to understand how visitors interact with the website. These cookies help provide information on metrics the number of visitors, bounce rate, traffic source, etc.
Advertisement
Advertisement cookies are used to provide visitors with relevant ads and marketing campaigns. These cookies track visitors across websites and collect information to provide customized ads.
Others
Other uncategorized cookies are those that are being analyzed and have not been classified into a category as yet.
SAVE & ACCEPT